Évolution plutonique et structurale de la presqu'île d'Akuliaruseq, Groenland méridional

Authors

  • F Persoz

DOI:

https://doi.org/10.34194/bullggu.v72.6610

Abstract

The Akuliaruseq area, situated between Julianehåb and Nanortalik, is formed of granites (ca. 75 % of the area) and gneisses belonging to the Canadian-Greenlandic shield. The geological history is divided into five periods of varying significance.

Cover image for volume 72

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Published

1969-02-26

How to Cite

Persoz, F. (1969). Évolution plutonique et structurale de la presqu’île d’Akuliaruseq, Groenland méridional. Bulletin Grønlands Geologiske Undersøgelse, 72, 1–202. https://doi.org/10.34194/bullggu.v72.6610

Issue

Vol. 72 (1969): Évolution plutonique et structurale de la presqu'île d'Akuliaruseq, Groenland méridional

Section

Monograph

License

This article is distributed under a CC-BY 4.0 licence, permitting free redistribution and reproduction for any purpose, even commercial, provided proper citation of the original work. Author(s) retain copyright over the article contents.